旱区覆膜滴灌棉田N 2 O排放对化肥减量有机替代的响应

覆膜滴灌条件下,采用静态箱-气相色谱法研究了不同施肥策略:CK(不施肥)、CF(N 300 kg/hm~2;P2O590 kg/hm~2;K2O 60 kg/hm~2)、60%CF+OF(普通有机肥6 000 kg/hm~2)、60%CF+BF(生物有机肥6 000 kg/hm~2)对棉田土壤N_2O排放的影响,旨在明确滴灌棉田连续不同施肥策略下土壤N_2O的排放特征。结果表明,棉花生育期N_2O排放通量表现为施肥处理大于不施肥处理,滴灌施肥后第3/4天N_2O排放通量顺序为CF60%CF+OF60%CF+BFCK,而滴灌后第7/8天N_2O排放通量则表现为有机肥处理高于化肥处理,滴灌施肥结束后表现与之相同;生育期的N_2O排放总量以100%化肥处理(CF)最高,与其相比,60%CF+OF和60%CF+BF处理分别降低3.75%和8.37%,N_2O排放系数则分别降低1.39%和73.8%;相关及通径分析均表明,与土壤NH+4-N相比,NO-3-N与N_2O排放的关系更密切。     

一种含有竹叶黄酮的复配型肉类食品添加剂的开发

通过竹叶黄酮和异Vc钠的系列复配应用试验,得到了一种性能优越的肉类食品添加剂.实验选用中式香肠体系,通过测定过氧化值(POV)、酸价(AV)和亚硝酸盐含量,辅以感官评定等手段,评价此复合抗氧化剂的抗氧性能以及对产品风味和质量的整体影响.结果表明,在原配方的基础上,硝酸盐或亚硝酸盐减半使用,同时添加0.01%的竹叶黄酮和0.05%的异Vc钠,能显著抑制香肠的脂质过氧化,延长产品保质期,降低产品中亚硝酸盐的含量,同时维持并改善中式香肠应有的感官品质.竹叶黄酮在有效发挥抗氧化作用的同时,部分替代了具有潜在致癌作用的发色剂,提高了制品的安全性,是一种十分有前途的肉类食品添加剂.     

巨大芽孢杆菌MPF-906对养鱼水质净化的初步研究

以鲫鱼为对象,利用从水产养殖水体中分离得到的巨大芽孢杆菌MPF-906,研究了其微生态制剂同步净化养鱼水质的动态变化。结果显示,在水族箱中添加巨大芽孢杆菌MPF-906制剂后,与对照组相比,水中的亚硝酸盐显著降解,COD也有所下降,pH值稳定在7.78￣8.19之间,表明巨大芽孢杆菌微生态制剂对净化养鱼水质和调节养殖水体微生态结构稳定具有明显的作用,其最适使用浓度为4×108CFU/mL。     

氨氮和亚硝酸氮对南美白对虾的毒性研究

用通常的生物毒性试验方法进行了氨氮和亚硝氨氮对体长5cm南美白对虾的急性毒性试验。在海水pH8.15、水温T＝27℃、盐度S＝20．0‰条件下，求得了两种物质对南美白对虾24h、48h、72h、96h的半死浓度，提出总氨氮和非离子氨氮对南美白对虾的安全浓度分别为2．667mg/L和0．201mg/L，亚硝酸氮的安全浓度为5．551mg/L。氨氮对南美白对虾的毒性强于亚硝酸氮，并提出降低氨氮和亚硝酸氮含量的措施。     

池塘中亚硝酸盐对草鱼种的毒害及防治

亚硝酸盐对草鱼种有很高的毒性,特别是水温超过30℃以上时。它主要是诱导草鱼血液中的血红蛋白转变为高铁血红蛋白,高铁血红蛋白超过血红蛋白总量的23.0％时,容易诱发草鱼出血病。随着草鱼血液中高铁血红蛋白的增高,红细胞数量和血红蛋白含量逐渐减少。池中亚硝酸盐氮含量到0.099±0.03毫克/升时,草鱼会出现出血病。清除水中亚硝酸盐氮的方法是在池塘中施加次氯酸钠,亚硝酸盐氮超过0.15毫克/升时,最好在池塘中先施加熟石灰,然后施加次氯酸钠,且以分次施用,效果较好。     

模拟胃液条件下假蒟叶提取物抑制亚硝化反应的研究

[目的]研究不同溶剂的假蒟叶提取物对亚硝化反应的影响。[方法]在模拟胃液条件下,测定假蒟叶提取物亚硝酸盐清除率及亚硝胺合成阻断率。[结果]不同溶剂的假蒟提取物均有一定的抑制亚硝化反应作用,其中乙酸乙酯提取物的抑制作用最强,且其对亚硝酸盐的清除率及对亚硝胺合成的阻断率在一定的浓度范围内随其浓度的增加而增加,对亚硝酸盐清除能力较强,其IC50值为0.425mg/ml,对亚硝胺合成阻断的能力相对较低,其IC50值为4.064 mg/ml。[结论]假蒟叶提取物具有较好的亚硝化反应抑制活性且主要通过清除底物亚硝酸盐来实现。     

山羊亚硝酸盐中毒口液,尿液,棉签偶氮显色快速诊断方法的研究

建立山羊亚硝酸盐中毒模型，用棉签分别蘸取口液、尿液立即滴加偶氮试剂均显粉红色，中毒后１０～２０ｍｉｎ显浅粉红色；６０ｍｉｎ显深粉红色，随中毒症状加重，棉签显色相应加深，甚致变为棕红色。同时棉签显色加深和血液褐变程度加重与ＭＨｂ／Ｈｂ比值升高同步。此种诊断方法是诊断亚硝酸盐中毒的动物可靠、灵敏和快速的诊断方法。     

Influence of thiosulfate on nitrification,denitrification, and production of nitric oxide and nitrous oxide in soil

Thiosulfate and CS₂ inhibit nitrification. The effect of the addition of thiosulfate on the turnover of inorganic N compounds was tested in an Egyptian and a German arable soil under nitrifying and denitrifying conditions. For nitrification, the soils were amended with NH _inf4 ^sup+ and incubated under aerobic conditions. For denitrification, the soils were amended with NO _inf3 ^sup- and incubated under anaerobic conditions. In both cases, the thiosulfate decreased with time while tetrathionate accumulated to an intermediate extent. Both compounds disappeared completely after <25 days. Production of CS₂ was not observed. Carbonyl sulfide was produced only in the Egyptian soil, but production decreased with increasing amounts of added thiosulfate. Under nitrifying conditions, the addition of increasing amounts of thiosulfate (25, 50, and 100 g S g^-1 dry weight) resulted in decreasing rates of NH _inf4 ^sup+ oxidation to NO _inf3 ^sup- ; it also resulted in an increasing intermediate accumulation of NO _inf2 ^sup- and NO, and in an increasing production of N₂O. Under denitrifying conditions, the addition of increasing amounts of thiosulfate did not significantly affect the rate of NO _inf3 ^sup- reduction, and resulted in an increasing intermediate accumulation of NO _inf2 ^sup- and of NO only in the German soil in which the production of N₂O was slightly inhibited by thiosulfate. These results demonstrate that the nitrification of NH _inf4 ^sup+ and NO _inf2 ^sup- was inhibited by increasing concentrations of thiosulfate and/or tetrathionate without involving the formation of volatile S compounds as potential nitrification inhibitors. Denitrification was not affected by the addition of thiosulfate.     

Denitrification and fermentation in plant-residue-amended soil

Summary Nitrous oxide production (denitrification) during anaerobic incubation of ground-alfalfa-, red-clover-, wheat-straw-, and cornstover-amended soil was positively related to the initial water-soluble C content of the residue- amended soil. The water-soluble C concentration decreased in all treatments during the first 2 days, then increased in the alfalfa-, red-clover-, and wheat-straw-amended soil until the end of the experiment at 15 days. An accumulation of acetate, propionate, and butyrate was partly responsible for the increased water-soluble C concentration. Denitrification rates were much higher in the alfalfa-and red-clover-amended soil, but NO ₃ ^– was not fully recovered as N₂O in these treatments. Supported by earlier experiments in our laboratory, we conclude that some of the NO ₃ ^– was reduced to NH ₄ ⁺ through fermentative NO ₃ ^– reduction, otherwise known as dissimilatory NO ₃ ^– reduction to NH ₄ ⁺ . Acetate, the primary product of anaerobic fermentation, accumulated in the alfalfa- and red-clover-amended soil in the presence of NO ₃ ^– , supporting previous observations that the processes of denitrification and fermentation occur simultaneously in C-amended soil. The partitioning of NO ₃ ^– between denitrification and fermentative NO ₃ ^– reduction to NH ₄ ⁺ depends on the activity of the denitrifying and fermentative bacterial populations. NO₂ concentration may be a key in the partitioning of NO ₃ ^– between these two processes.     

Ammonium oxidation coupled to dissimilatory reduction of iron under anaerobic conditions in wetland soils

In exploring the dynamics of iron and nitrogen cycling in sediments from riparian forests we have observed a redox reaction that has not been previously described. During incubations of soil slurries under strictly anaerobic conditions, we repeatedly measured an unexpected production of both nitrite () and ferrous iron [Fe(II)]. Using this indirect evidence we hypothesize that, under anaerobic conditions, there is a biological process that uses ferric iron [Fe(III)] as an electron acceptor while oxidizing ammonium () to for energy production. This oxidation under iron reducing anaerobic conditions is thermodynamically feasible and is potentially a critical component of the N cycle in saturated sediments.